Predictable zone for phase-resolved reconstruction and forecast of irregular waves
Our interest is the phase-resolved reconstruction and forecast of multidirectional irregular gravity wave fields based on specific wave measurements. We consider the theoretical predictable zone P in space–time within which the phase-resolved wave field can be fully reconstructed/forecasted based on...
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Published in | Wave motion Vol. 77; pp. 195 - 213 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.03.2018
Elsevier BV |
Subjects | |
Online Access | Get full text |
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Summary: | Our interest is the phase-resolved reconstruction and forecast of multidirectional irregular gravity wave fields based on specific wave measurements. We consider the theoretical predictable zone P in space–time within which the phase-resolved wave field can be fully reconstructed/forecasted based on the given measurements. Using linearized wave theory and reasonable assumptions of the frequency and directional extent of the wave field, we obtain closed-form expressions for P in terms of set theory expressions involving the individual measurement. We derive and illustrate P obtained for measurements at one or more fixed locations over time, for moving probes, for whole-area wave measurements, and combinations of these. We also consider the problem of optimal deployment of these measurements to maximize the volume of P in space–time. For J probes under optimal deployment, we show that the volume of P relative to that of a single probe scales as J3 for large J.
•Phase-resolved predictable zone of irregular waves for given measurements is derived.•The predictable zone is derived in closed-form expression based on linearized wave theory.•Measurements can be one or more fixed/moving probes and/or whole-area measurements.•Optimal deployment of measurements to maximize the predictable zone is derived.•Asymptotic estimate of predictable zone volume for large number of measurements is obtained. |
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ISSN: | 0165-2125 1878-433X |
DOI: | 10.1016/j.wavemoti.2017.12.001 |